Atmospheric water transport connectivity within and between ocean basins and land
The global atmospheric water transport from the net evaporation to the net precipitation regions has been traced using Lagrangian trajectories. A matrix has been constructed by selecting various group of trajectories based on their surface starting (net evaporation) and ending (net precipitation) po...
Published in: | Hydrology and Earth System Sciences |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2023
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Online Access: | https://doi.org/10.5194/hess-27-481-2023 https://doaj.org/article/ce754d1076b94f59b92c9013b40dbd1d |
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author | D. Dey A. Aldama Campino K. Döös |
author_facet | D. Dey A. Aldama Campino K. Döös |
author_sort | D. Dey |
collection | Directory of Open Access Journals: DOAJ Articles |
container_issue | 2 |
container_start_page | 481 |
container_title | Hydrology and Earth System Sciences |
container_volume | 27 |
description | The global atmospheric water transport from the net evaporation to the net precipitation regions has been traced using Lagrangian trajectories. A matrix has been constructed by selecting various group of trajectories based on their surface starting (net evaporation) and ending (net precipitation) positions to show the connectivity of the 3-D atmospheric water transport within and between the three major ocean basins and the global landmass. The analysis reveals that a major portion of the net evaporated water precipitates back into the same region, namely 67 % for the Indian Ocean, 64 % for the Atlantic Ocean, 85 % for the Pacific Ocean and 72 % for the global landmass. It has also been calculated that 58 % of the net terrestrial precipitation was sourced from land evaporation. The net evaporation from the subtropical regions of the Indian, Atlantic and Pacific oceans is found to be the primary source of atmospheric water for precipitation over the Intertropical Convergence Zone (ITCZ) in the corresponding basins. The net evaporated waters from the subtropical and western Indian Ocean were traced as the source for precipitation over the South Asian and eastern African landmass, while Atlantic Ocean waters are responsible for rainfall over North Asia and western Africa. Atlantic storm tracks were identified as the carrier of atmospheric water that precipitates over Europe, while the Pacific storm tracks were responsible for North American, eastern Asian and Australian precipitation. The bulk of South and Central American precipitation is found to have its source in the tropical Atlantic Ocean. The land-to-land atmospheric water transport is pronounced over the Amazon basin, western coast of South America, Congo basin, northeastern Asia, Canada and Greenland. The ocean-to-land and land-to-ocean water transport through the atmosphere was computed to be 2×10 9 and 1×10 9 kg s −1 , respectively. The difference between them (net ocean-to-land transport), i.e. 1×10 9 kg s −1 , is transported to land. This net transport ... |
format | Article in Journal/Newspaper |
genre | Greenland |
genre_facet | Greenland |
geographic | Canada Greenland Indian Pacific |
geographic_facet | Canada Greenland Indian Pacific |
id | ftdoajarticles:oai:doaj.org/article:ce754d1076b94f59b92c9013b40dbd1d |
institution | Open Polar |
language | English |
op_collection_id | ftdoajarticles |
op_container_end_page | 493 |
op_doi | https://doi.org/10.5194/hess-27-481-2023 |
op_relation | https://hess.copernicus.org/articles/27/481/2023/hess-27-481-2023.pdf https://doaj.org/toc/1027-5606 https://doaj.org/toc/1607-7938 doi:10.5194/hess-27-481-2023 1027-5606 1607-7938 https://doaj.org/article/ce754d1076b94f59b92c9013b40dbd1d |
op_source | Hydrology and Earth System Sciences, Vol 27, Pp 481-493 (2023) |
publishDate | 2023 |
publisher | Copernicus Publications |
record_format | openpolar |
spelling | ftdoajarticles:oai:doaj.org/article:ce754d1076b94f59b92c9013b40dbd1d 2025-01-16T22:13:53+00:00 Atmospheric water transport connectivity within and between ocean basins and land D. Dey A. Aldama Campino K. Döös 2023-01-01T00:00:00Z https://doi.org/10.5194/hess-27-481-2023 https://doaj.org/article/ce754d1076b94f59b92c9013b40dbd1d EN eng Copernicus Publications https://hess.copernicus.org/articles/27/481/2023/hess-27-481-2023.pdf https://doaj.org/toc/1027-5606 https://doaj.org/toc/1607-7938 doi:10.5194/hess-27-481-2023 1027-5606 1607-7938 https://doaj.org/article/ce754d1076b94f59b92c9013b40dbd1d Hydrology and Earth System Sciences, Vol 27, Pp 481-493 (2023) Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 article 2023 ftdoajarticles https://doi.org/10.5194/hess-27-481-2023 2023-01-29T01:30:11Z The global atmospheric water transport from the net evaporation to the net precipitation regions has been traced using Lagrangian trajectories. A matrix has been constructed by selecting various group of trajectories based on their surface starting (net evaporation) and ending (net precipitation) positions to show the connectivity of the 3-D atmospheric water transport within and between the three major ocean basins and the global landmass. The analysis reveals that a major portion of the net evaporated water precipitates back into the same region, namely 67 % for the Indian Ocean, 64 % for the Atlantic Ocean, 85 % for the Pacific Ocean and 72 % for the global landmass. It has also been calculated that 58 % of the net terrestrial precipitation was sourced from land evaporation. The net evaporation from the subtropical regions of the Indian, Atlantic and Pacific oceans is found to be the primary source of atmospheric water for precipitation over the Intertropical Convergence Zone (ITCZ) in the corresponding basins. The net evaporated waters from the subtropical and western Indian Ocean were traced as the source for precipitation over the South Asian and eastern African landmass, while Atlantic Ocean waters are responsible for rainfall over North Asia and western Africa. Atlantic storm tracks were identified as the carrier of atmospheric water that precipitates over Europe, while the Pacific storm tracks were responsible for North American, eastern Asian and Australian precipitation. The bulk of South and Central American precipitation is found to have its source in the tropical Atlantic Ocean. The land-to-land atmospheric water transport is pronounced over the Amazon basin, western coast of South America, Congo basin, northeastern Asia, Canada and Greenland. The ocean-to-land and land-to-ocean water transport through the atmosphere was computed to be 2×10 9 and 1×10 9 kg s −1 , respectively. The difference between them (net ocean-to-land transport), i.e. 1×10 9 kg s −1 , is transported to land. This net transport ... Article in Journal/Newspaper Greenland Directory of Open Access Journals: DOAJ Articles Canada Greenland Indian Pacific Hydrology and Earth System Sciences 27 2 481 493 |
spellingShingle | Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 D. Dey A. Aldama Campino K. Döös Atmospheric water transport connectivity within and between ocean basins and land |
title | Atmospheric water transport connectivity within and between ocean basins and land |
title_full | Atmospheric water transport connectivity within and between ocean basins and land |
title_fullStr | Atmospheric water transport connectivity within and between ocean basins and land |
title_full_unstemmed | Atmospheric water transport connectivity within and between ocean basins and land |
title_short | Atmospheric water transport connectivity within and between ocean basins and land |
title_sort | atmospheric water transport connectivity within and between ocean basins and land |
topic | Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 |
topic_facet | Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 |
url | https://doi.org/10.5194/hess-27-481-2023 https://doaj.org/article/ce754d1076b94f59b92c9013b40dbd1d |